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济宁地区北部岩溶地下水资源计算与潜力评价 总被引:1,自引:1,他引:0
济宁地区北部赋存有较丰富的岩溶地下水,目前已纳入当地开发利用规划。为防止过量开采引发不良环境地质问题,对该岩溶系统的资源潜力进行了科学评价。在查明济宁地区北部水文地质条件的基础上,利用水量均衡法与数值模拟法对该区岩溶地下水资源量进行了计算,通过分析地下水资源潜力模数,该区岩溶地下水资源潜力较大。 相似文献
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地下水是一个城市水循环的重要组成部分,地下水的质量关系到城市居民的生命健康安全.为确定济南地区地下水的污染状况,本文以历年的水文资料作为背景值,采用了单因子和多因子2种评价方法对济南地区岩溶水进行了污染程度评价,根据评价结果将研究区岩溶水污染程度进行了分级;在地下水系统防污性方面,采用DRASTIC模型对济南地区的防污... 相似文献
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文章通过对广西岩溶发育特征与地下水的分布规律和赋存条件进行研究,提出广西岩溶地下水源地类型划分方案,并对不同类型的岩溶水源地开发技术条件进行介绍。 相似文献
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曲潭测区内地形较平坦,多为第四系覆盖,表层土质较均匀,接地条件较好,选择五极纵轴电测深法在区内寻找岩溶地下水,通过视电阻率及激电二次场的测量,对物探异常的解译和深部钻孔验证,成功找到日出水量达千吨以上的岩溶地下水,为今后在灰岩地区寻找岩溶地下水提供借鉴意义。采用物探方法寻找岩溶地下水是一种不可替代的勘查方法,可以减少单纯钻探成井的盲目性,提高找水的成功率。 相似文献
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综合分析沂南县气候、自然、地理,尤其是地质与水文地质条件,及2011年国土资源抗旱打井工作成果,结合沂南地下水含水岩组分布、赋存、地下水运移特征、构造对岩溶发育与地下水运动的控制等。得出沂南县岩溶地下水补给径流区的构造破碎带及其附近地下水相对富集。地下水富集特征可分为:构造带控水型、火成岩体阻挡富水型、断裂影响带强富水型及远离构造破碎带弱富水型等几种类型。根据岩溶地下水补给径流区地下水富集规律的分析研究,为今后贫水山区找水定井提供参考。 相似文献
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莒县灰岩地层产状较陡,多被断裂切割成若干个SN向窄条带状分布的小块段,岩溶发育具有不均一性,地下水资源缺乏,灰岩地层富水性研究对当地水源供给保障具有重要意义。本文以龙王庙富水块段为例,依据"1∶5万东莞幅、招贤幅区域水文地质调查"的实际调查分析数据,系统地进行富水性研究,从地形地貌、地层岩性、地质构造以及地下水动力条件4个方面分析岩溶地下水富集规律,认为只要在这4个方面具备有利条件,就有较大可能形成相对富水块段。该次在灰岩地区找水的成功经验,对于今后在其他灰岩地区开展找水工程及相关研究具有一定的借鉴意义。 相似文献
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华北平原水资源紧缺情势与因源 总被引:15,自引:0,他引:15
基于水资源可持续利用理念,从水资源承载能力演化周期性、经济社会需用水规模难变性和未来水资源供需关系入手,介绍近60年以来华北平原水资源情势,特别是该平原水资源量、实际用水量和地下水开采量变化特征,并结合未来10到30年区域经济社会发展需用水量趋势,识别和诊断华北平原水资源紧缺因源.结果表明:由于降水量减少导致华北平原缺... 相似文献
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Wang Lilun 《中国地理科学(英文版)》1996,6(4):304-312
THE CONDITIONS OF THE GLACIAL WATER RESOURCE AND WAYS OF ITS EXPLOITATION AND UTILIZATION IN CHINATHECONDITIONSOFTHEGLACIALWA... 相似文献
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面向新时期水利行业"补短板"和"强监管"的应用需求,遥感的前沿技术高光谱遥感凭借较高的光谱分辨率和图谱合一等优势,在水生态、水环境等水利行业的应用中发挥了重要作用,同时在水灾害、水资源等层面中也存在着一定的应用潜力.本文介绍了高光谱遥感的成像原理,回顾了成像光谱仪的发展,列举了目前国内外典型的高光谱载荷.重点介绍了高光... 相似文献
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Zhang Ji-shi Zhang Yong-qiu Pu Rui-feng Chen Ren-sheng Cheng Zhong-shan Wang Ming-quan 《中国地理科学(英文版)》2005,15(3):238-244
The research on the present situation of soil and water development and utilization in Shiyang River Basin shows that water
resources and eco-environment situation in this area are near the edge of collapse. Since the water crises occurred in the
1970s, problems caused by continuous decrease of water resources have been becoming serious year by year and eco-environment
crisis occurred as a consequence. Up to now, 10 380ha of irrigated lands have been abandoned due to sand coverage and water
shortage in the basin. Ground water was over exploded in Wuwei and Minqin because of water shortage. Ground water table in
many places dropped under 5m (which is the ecology water table level), thus about 3000ha of Elaeagnus angustifolia forest come to dead and another 5800ha become feeble, and wind-drift sand near the oasis become alive. According to the current
situation, if water utilization scope was not enlarged, a water transfer volume of 600×106m3/a from other areas will be suitable to keep water resources and eco-environment safety in the basin, and also 70×106m3/a will be left as spare water. Under this condition the water resources and eco-environment of the basin can reach the critical
safety line of 2.032×109m3/a; or if 180×106m3 of water can be transferred from other areas, the water resources can reach the safety warning line of 1.732×109m3/a.
Foundation item: Under the auspices of the National Natural Science Foundation of China (No. 40235053) and Lanzhou Jiaotong
University "Qinglan" Foundation
Biography: ZHANG Ji-shi (1963-), male, a native of Tongwei of Gansu Province, senior engineer, specialized in water resources
and climate change in Northwest China. E-mail: zjs1963@yahoo.com.cn; hangjs@mail.lzjtu.cn 相似文献
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North China, whose total area is 420,000 km2, covers 2 provinces and 2 cities (Shanxi and Hebei provinces, Beijing and Tianjin) and the territories of Henan and Shandong provinces to the north of the Huanghe (Yellow) River, and part of the Inner Mongolia Autonomous Region and Liaoning Province. Most of this region, which is situated in the semi-humid, semi-arid continental climate temperate zone, gets an annual precipitation of 500-600 mm, whereas, the perennial average amount of total water resource is 50.99 billion m3, including 33.82 billion m3 of surface water, 32.94 billion m3 of ground water and 15.77 billion m3 of their duplication. Due to the intensive exploitation of water resource caused by the deficiency of water resource in North China, key elements of water balance was changed, runoff volume reduced, evaporation increased, vertical movement of moisture strengthened, water circulation pattern transformed from open system into regionally closed system; meanwhile, due to the incompetent water 相似文献
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Riverwaterresourceisthemostimportantcom ponentofwaterresourcesinChina .ComprehensiveandspecificresearchesonriverwaterchemistryinChinahavebeencarriedoutsincethe 1950s.Theob jectiveofthispaperistoreviewtheprogressintheresearchonriverwaterchemistryinChina ,es… 相似文献
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The processes of water resources exploitation and utilization can be divided into three stages by water resources transformation,
and the history, present situation and future trend of water resources development in piedmont areas around high mountains
of arid northwestern China. The three stages are: the stage of surface water development (the first stage), the stage of comprehensive
development of surface and ground water (the second stage) and the stage of economical development of water resources (the
third stage). The three stages link each other and show the law and processes of water resources exploitation and utilization
associated with social and technological progress. The economical water policy should run through the three stages. On this
point, however, the third stage differs from the others, particularly, refering to irrigated agriculture. The third stage
has more progressive significance because it breaks the traditional ideas on water resources development. According to our
investigation and calculation, under present conditions of water resources development, the net used water is about 160 ×
108 m3, accounting for 18% of the total water resources of northwestern China. The water resources have not been fully developed.
If the first stage is finished, the exploitable water can be increased by 91%. After the second stage, furthermore, it can
be increased by 216%.
Supported by the National Natural Science Foundation of China. 相似文献